Proportional Nomograms - WordPress.com · 2016. 8. 29. · and a line parallel to the grid is...

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Proportional Nomograms True for all types shown here Proportional Design: 4 Variable Proportion Other Layouts

Transcript of Proportional Nomograms - WordPress.com · 2016. 8. 29. · and a line parallel to the grid is...

  • Proportional Nomograms

    True for all types shown here

    Proportional Design:

    4 Variable Proportion

    Other Layouts

  • Father’s Day

  • Mother’s Day

    Memorial Day

  • Compound Linear Design:

    Compound Nomograms

    Equations of more than three variables can be graphically computed using compound nomograms sharing scales.

    k

    Themiddlesolutionscaleoftheconcurrentnomogram

    fortworesistorsinparallelcanbeusedastheouter

    scaleofasecondnomogramtoextendthenomogram

    forthreeresistors.Afourthparallelresistorcanbe

    addedbyseesawingbackthroughthefirstsetof

    scales,andsoforth.Aseriesresistorsimplyslides

    upwardalongthescale.

    Since the angle A between the

    scales is 60, the scales are

    identical.

    The k-scale is not labeled with scale

    values. It is called a pivot line.

  • Two Classic Nomogram Designs

    A Concurrent-Scale Nomogram

    where A is the angle between each of the 3 scales.

    If A = 60° as below, then m1 = m2 = m3.

    Standard resistor values can be marked so

    a convenient combination can be found by

    playing with the straightedge.

    Here we have

    r2 = V/πh

    An “N” or “Z” ChartDesign:

    The diagonal scale can be floating segment,

    thus appearing “rather more spectacular” to

    the casual observer [Douglass 1947].

    Design:

    Division Harmonic Relation

  • Independence Day Independence Day (Obs.)

  • Easter Sunday

  • Solving Polynomial EquationsFinding real roots graphically

    Linear scales and

    easy custom ranges

    of A and B for

    Ax2+ x + B = 0

    No need to

    graduate the

    circle! Read the

    roots as –B on

    lines from O

    through the

    marked location

    on the circle

    (here -3.06 for

    A=-0.1, B=4)

    Wheeler, The Mathematical

    Gazette, 41:336, May, 1957

    Two real roots are found if the isopleth cuts the circle,

    one repeated real root if it touches the circle, no real

    roots if it misses the circle entirely

    For a real root w1found here,

    the second root = u+w1

    Not a nomogram, but a networkor

    intersectionchartfor finding roots of the

    cubic equation z3+ pz+ q = 0. There will

    be one real root, 3 real roots of which

    two are equal, or 3 real roots, depending

    on whether z (interpolated between the

    slanted lines) lies outside of the

    triangular region, on its boundary, or

    within it. For example, p=0.6 and q=-0.4

    gives z=0.47, while p=-0.8 and q=0.11

    gives z=-0.96, 0.82, 0.14.

    q2–aq + b = 0

    w2+ uw + v = 0

  • Nomography

    The simplicity of a

    nomogram can be

    startling!

    Much simpler to plot

    No family of curves or

    grid

    Much finer resolution

    Less prone to

    mistakes

    Can be extended to

    additional variables

    A straightedge

    (such as the

    edge of a sheet

    of paper or a

    string) called an

    isopleth is used

    to connect

    known values to

    find the

    unknown value.

    Nomograms solve equations in 3 or more variables, providing lightning fast, easy calculations to an engineering precision in a form that is easy to reproduce on a photocopier

    T = 1.0

    T = 1.1

    T = 1.2

    T = 1.3

    T = 1.4

    T = 1.5

    T = 1.6

    T = 1.7

    T = 1.8

    T = 1.9

    T = 2.0

    A traditional three-variable graph

    A parallel-scale nomogram

    Example: N = (1.2D + 0.47)0.68(0.91T)3/2Nomography was invented in 1880 by Maurice d’Ocagne and was used extensively for many years to provide engineers with fast graphical calculations of complicated formulas to a practical precision.

    Parallel-Scale Design:

    m1 = height/range for D scale

    m2 = height/range for T scale

    m3 = m1m2/(m1+m2)

    a/b = m1/m2 and a+b =

    width0.68 log(1.2D + 0.47) + 1.5 log T = log N – 1.5 log 0.91

    Take logarithms to convert the equation t0 a sum

  • AstronomyOnce invented, nomogramswere soon applied to time-consuming and repetitive calculations in celestial mechanics

    This is an example of a

    nomogram solving for a

    variable (φ) that cannot be

    isolated algebraically.

    nt = φ–e sin φ

    Kepler’sEquation for the relation between the

    polar angle φof a celestial body in an eccentric

    orbit and the time elapsed from an initial point

    Celestial Parallax: the difference between

    topocentric and geocentric location when

    observing comets and minor planets. Done

    with parallax correction, generally to two

    digits and in great number to define the

    orbits:

    Δpα= parallax factor

    πs = mean equatorial horizontal

    parallax of the sun in seconds

    ρ= Earth radius to observation

    point in term of equatorial radius

    φ= geocentric latitude of

    observer

    δ,H = declination and hour angle

    of body

    Kresàk, Bulletin of the

    Astronomical Institute of

    Czechoslovakia, 1957

    after Leif Roschier—see

    http://www.pynomo.org/wiki/index.php/Example:Star_navigation

    Spherical Triangle relation between

    declination, latitude, hour angle and azimuth

    Spherical Triangle relation between

    declination, latitude, altitude and azimuth

  • Dygograms

    Now extend ND the same distance beyond

    D to find the South (S) point. The point Q is

    the intersection with the circle. Continue to

    create the Limaçon of Pascal figure by

    moving the midpoint of the segment NS

    along the circle and marking the endpoints.

    δ = A + B sin ζ’ + C cos ζ’ + D sin 2 ζ’ + E cos ζ’

    For any ship compass

    reading (the compass

    course ζ’), draw a line

    from Q at this angle

    from QN (the red

    arrow here) and mark

    the point where it

    crosses the vertical

    line OX. Then with

    dividers construct an

    arc that passes

    through O, Q, and this

    point (the blue circle)

    and mark a new point

    where it crosses the

    limaçon (the magnetic

    course ζ). The

    magnetic deviation δ is

    the angle between OX

    and this new point as

    read on the protractor.

    δ is the magnetic deviation (compass correction)

    ζ’ is the ship compass reading (compass course)

    A, D, E, λ, c, f, P and Q are magnetic parameters

    measured for the ship

    H and θ are the horizontal component and dip angle

    of the Earth’s magnetic variation at the ship location

    A = arcsin A

    B = arcsin [B / (1 + ½ sin D)]

    C = arcsin [C / (1 - ½ sin D)]

    D = arcsin D

    E = arcsin E

    A, D, E = constants for ship

    B = (1/λ) (c tan θ + P / H)

    C = (1/λ) (f tan θ + Q / H)

    The Scottish mathematician and lawyer Archibald Smith first published in 1843 his equations for the magnetic deviation of a ship, or in other words, the error in the ship’s compasses from permanent and Earth-induced magnetic fields in the iron of the ship itself. This effect had been noticed in mostly wooden ships for centuries, and broad attempts to minimize it were implemented. But the advent of ships with iron hulls and steam engines in the early 1800s created a real crisis. A mathematical formulation of the deviation for all compass courses for a location at sea was needed in order to understand and compensate for it. Smith invented graphical methods for quickly calculating the magnetic deviation for any ship’s course once ship parameters were found, geometric constructions called dynamogoniograms (force-angle diagrams), or dygograms for short.

    To construct a dygogram, find the

    North (N) position by laying out from O

    the lengths A, B, C, D and E as

    shown. Draw a circle centered at A

    and passing through D. The magnetic

    deviation δ for a magnetic course ζ of

    North (0 ) is the angle XON read on

    the protractor.

    Alternate graphical computers

  • Labor Day

  • Valentine’s DayPresident’s Day

  • Navigation and Surveying

    Friauf, Am. Math.

    Monthly, 42:4, 1935

    A 3D (4x4 determinant) nomogram

    solution for Great Circle Distance

    Here the φ-scale lies the same distance dabove the paper as the L-scale lies

    below it, but they are flattened to the paper.First, points A and B are joined by a

    line. Then for a given L (point C), all four points will be coplanar if the point on the

    flattened φ-scale is the same distance from AB as C and on a line parallel to AB.

    A transparent overlay of parallel lines is used to find φ.

    M. Collignon

    sin φ–cos φtan ε–ρtan ε= 0

    Angular correction for land surveys

    Great Circle Distance

    λ–λ’ = 25.2 °

    λ+ λ’ = 72.5 °

    L = 116 °

    φ= 87.5°

  • Lallemand’s L’Abaque Triomphe

    In 1885, Charles Lallemand, director

    general of the geodetic measurement of

    altitudes throughout France, published a

    hexagonal chart for determining the

    compass course correction (the magnetic

    deviation) due to iron in the ship, Le

    Triomphe for any navigable location on

    Earth. It is a stunning piece of work,

    combining measured values of magnetic

    variation around the world with eight

    magnetic parameters of the ship also

    measured experimentally, all merged into a

    very complicated formula for magnetic

    deviation as seen at the top of the chart.

    The sample calculation on the chart is described above:

    1. The ship latitude and longitude is located among the curved lines on the leftmost map and a horizontal line is

    extended to the compass course ζ’ in the center hourglass grid (a distance Y1 = B sin ζ’ from the vertical green line)

    2. The ship latitude and longitude is found in the upper (for a northerly heading) or lower (for a southerly heading) map

    and a line parallel to the grid is extended to the corresponding compass course in the twisted grid (a distance Y2 = A +

    C cos ζ’ + D sin 2 ζ’ + E cos ζ’ from the angled green line).

    3. A translucent hexagonal overlay (shown in blue) is overlaid so that two arms pass through the two marked points.

    Through a geometric exercise, it can be shown that the magnetic deviation (compass correction) Y3 on the third scale

    is the sum of Y1 and Y2.

    ζ’ is the current ship compass reading ( or compass

    course)

    H and θ are the horizontal component and dip angle of

    the Earth’s magnetic variation at the ship location

    A, D, E, λ, c, f, P and Q are magnetic parameters

    measured for Le Triomphe

  • Columbus Day (Generally)

    Halloween

  • New Year’s Day

    Martin Luther King Day

  • Shared-Scale Nomograms

    Here the h1 and h2scales are identical, and two

    ranges are marked on different sides of the scales.

    f1(u)f2(v)f3(w) = 1

    The 3 real roots of a cubic

    equation ax3+bx2+cx+d = 0

    sum to –b/a, so a plot of x3

    marked with its x-values

    provides a single scale

    nomogram for addition.

    To generalize these from u, v, w to f1(u), f2(v), f3(w),

    we assign to the scales the values for which f1(u),

    f2(v) and f3(w) will provide the values we see here.

    With proper mathematical preparation, two or more scales can share a curve, or even share the same values on that curve

    f1(u) + f2(v) + f3(w) = f1(u)f2(v)f3(w)

    u+v+w = 0

  • Lalanne’s Universal Calculator

    LaLanne envisioned copies of his Universal

    Calculator posted in public squares and

    business meeting places for popular use.

    In 1844, Leon LaLanne created the first log-log plot in history, his Universal Calculator.

    The product of x and y is found from their intersection with the 45°lines, squares at the 45°line from the origin, cubes from the steeper (Cub) line from the origin or its wraparound, and various engineering and chemical formulas of roots and powers at their lines. Following the line to the edge continues a calculation to additional terms.

    Trigonometric functions are plotted along the sides for use (or use of their inverses) in calculations as well.

  • Election Day

    Veteran’s Day

    Thanksgiving

  • Introduction

    In 1844 Leon Lalanne succeeded in linearizing the curves y=xpby plotting the first log-log plot in history, thereby creating his Universal Calculator, chock-full of lines for common engineering calculations and capable of graphically computing formulas in powers or roots of x( or of trigonometric functions in x)with ease. The year 1844 is taken here as the start of the Age of Graphical Computing. Other graphical methods evolved, and ultimately the field of nomography was invented in 1880 by Maurice d’Ocagne, a breakthrough in graphical computing so radical that it dominated the field of graphical computing until the spread of computers and electronic calculators in the early 1970s.

    This 2010 calendar predominantly treats the field of nomography and the amazing variety of nomograms that can be created from it. A nomogram is a layout of graphical scales for computing formulas of 3 or more variables using a straightedge such as a ruler or the edge of a sheet of paper. A drawn or imagined isoplethconnects matching values

    Ron Doerfler

    [email protected]

    Nomograms can be created with geometric relations, but the more extraordinary ones are nearly always created using a method of determinants developed by d’Ocagne. Sometimes in this calendar you will see an equation adjacent to a nomogram, in which the determinant of a matrix is set equal to zero. When the determinant is expanded, you will see that the resulting equation matches the overall equation of the nomogram. If the determinant is in a form where no variable appears in more than one row and the last column is all 1’s, then the first two elements in each row represent the (x,y) location of the scale point for values of the variable(s) in that row. For example, using the rules for expanding a determinant the equation w= u/(u + v2+ 1) or uw + v2w + w –u = 0 can be expressed as

    so a tick on the u-scale lies at (0,u) for every u, (or in other words the u-scale is a linear, vertical scale), the ticks on the v-scale are at (1,-v2), and the ticks on the w-scale are at (w,w) resulting in a linear 45degree scale.

    Most of the nomograms herein were created with the PyNomo software package of Leif Roschier found at

    http://www.pynomo.org. The calendar pages are based on an InDesign template created by Juliana

    Halvorson at http://www.graphmaster.com/calendarinstructions/. All other content ©2010 Ron Doerfler

    of variables for a particular formula, so if all variables but one is known, the unknown variable can be read off the intersection of the isopleth with its scale. Variables that cannot be isolated algebraically can be read directly off a nomogram. Beyond their practical use,the scales of a nomogram often create geometric figures and curves of a certain beauty and flair, influenced to a striking degree by the cleverness of the nomographer. Simple nomograms can be seen today at times in engineering catalogs and medical offices, but the really creativeones, the ones that universally draw interest and display the wondrous virtuosity of mathematics, are nowhere to be found anymore.

    The nomograms in this calendar are representative of some of the variety once in use for graphical computing, but in no way doesit approach a significant survey of this rich field of study. Perhaps a 2011 calendar will consider other designs. Additional information on nomograms and other topics in this calendar can be found in articles on my blog, “Dead Reckonings: Lost Art in the Mathematical Sciences” at http://www.myreckonings.com/wordpress. I hope you have a happy year in 2010.

  • An Assortment of Nomograms

    Nomograms existed for a variety

    of vector and complex number

    calculations

    A compass is used here

    instead of a straightedge

    A projection transformation for

    greater accuracy at large X

    A rare instance of 4

    individual scales for a

    single isopleth

    sinh(A + jB) = p + jqRybner

    Hoelscher

    Meyer

    The θscale could

    actually stop at 45.

    For angles beyond

    this, θ90 –θand x

    and y are swapped.

  • Introduction

    It is difficult for us today to grasp the drudgery of complex arithmetic calculations, or even repeated simpler calculations, in the past. This was especially true with repetitive computations that required tables of roots, logarithms and trigonometric functions in such fields as astronomy, navigation, surveying, and a wide variety of military and engineering applications.

    Have you ever had to calculate the positions of astronomical objects? Orbital calculations relative to an observer on the Earth require derivations and time-consuming solutions of spherical trigonometric equations. And yet these kinds of calculations were accomplished by ancients such as Vitruvius and Ptolemy in the days prior to the advent of calculators or computers, or even trigonometry or algebra, using methods of Descriptive Geometry that are rarely taught today.

    The Greeks folded (rabatted) the fundamental great circles onto the page and performed intricate geometrical constructions to map the Earth-Sun relative motion and incorporate local measurements into global maps and sophisticated sundials.

    Astrolabes, quadrants and other volvelles and dials evolved to perform more complex computations in graphical form. In 1610-1614, Joost Bürgi and John Napier invented logarithms, and mathematicians and scientists such as Johann Kepler created tables of logarithms to aid in computation. William Oughtred and others developed the slide rule in the 1600s based on the properties of logarithms, and the slide rule continued its dominant role in non-graphical computation until the early 1970s. The slide rule provided the greatest versatility in computing the vast variety of equations, but it required multiple error-prone steps to provide solutions, effort that was not decreased even when solving one equation repetitively.

    Meanwhile, on the graphical front Rene Descartes created the Cartesian coordinate system in the 17th century, and mathematicians over the next two centuries laid the foundation for applied numerical mathematics in large part on this field of analytical geometry. A two-dimensional graph provided fast solutions to an engineering precision for a single equation in two variables, and more complicated families of curves or so-called intersection charts extended the use of Cartesian graphs to one additional variable. T = 1.0

    T = 1.1T = 1.2T = 1.3T = 1.4T = 1.5

    T = 1.6

    T = 1.7

    T = 1.8

    T = 1.9

    T = 2.0

  • Christmas DayChristmas Eve

    New Year’s Eve

  • The Age of

    A 2010 Calendar

    Graphical Computing y

    A.D. 1844 A.D. 1974

  • A 2010 Calendar of Graphical Computers

    As a calculating aid graphical computers can solve very

    complicated formulas with amazing ease.

    As a curiosity graphical computers manifest the beauty

    of mathematics in a highly visual, highly creative way.

    Graphical Computers are fascinating artifacts in the history of mathematics. They possess an intrinsic charm well beyond their practical use.

    Most of the nomograms herein were created with the PyNomo software package of Leif Roschier found

    at http://www.pynomo.org. The calendar pages are based on an InDesign template created by Juliana

    Halvorson at http://www.graphmaster.com/calendarinstructions/. All other content ©2010 Ron Doerfler

    Contact: [email protected]